360 DR. W. HIND AND MR. J. A. HOWE ON THE [Aug. I90I, 



Feet. Inches. 



Shales 15 



Sandy shales, with a 9-inch sandstone 9 



Gritty sandstone 9 



Sandstone 9 



Massive sandstone 12 



Flaggy shales, with Posidonomya Becheri 12 



Mudstone 8 



Shales 3 



Fine-grained sandstone 3 6 



Shale 9 



Sandstone 1 



Flaggy sandstone 18 



[At this point is the flood-rail in the stream.] 



Massive fine-grained sandstone 9 



Sandstone with shaly partings 3 



Shale 10 



Shale w ith thin sandstone 9 



Sandstone with boxstones 8 



Fine grey paper-shales 2 9 



Waterfall over massive sandstone 6 



Shaly parting 6 



Sandstone 8 



Shaly sandstone 6 



Compact sandstone 14 



Micaceous dark-grey sandstone 8 



Flaggy shales 4 



Grey paper-shales 9 



Black shales 10 



Lenticular bands of limestone 3 



Hard muddy shales I 



Fine shale I 15 



Gritty shale J 



Limestone, with crinoid-fragments 1 



Shales, with A viculojoecten papyraceus 6 



'L\me?X,onQyf\i\\PhilUpsia Van der Grachtii, Gonia- 

 titcs, three species of gasteropods, and a fish- 

 scale 



Black shales 6 



Limestone 3 



Calcareous shale 1 



Fossil-band 4 



Shale 3 



Limestone 2 



Shales with Aviculopecten papyraceus, Posidonomya 



Becheri, Fosidoniella l(svis, and Discites sp 6 



Gap 120 



Limestone-conglomerate, rolled shells and frag- 

 ments, Productus Cora, Spirifera, and corals. 



The last-mentioned, bed is so remarkably like the conglomerate 

 of Erockthorns and Pythorns, that the above section may be con- 

 sidered to give a very fair representation of the whole series between 

 the limestone-massif and the grits. 



In the becks on the western flank of Flashy Fell we find a typical 

 Pendleside sequence ; the massive limestone is not exposed here, 

 but its presence seems to be indicated by a strong feature running 



along the lower llank of the hill, and a gamekeeper told us that he 



